Mediterranean Climate Quotes

The technologies which have had the most profound effects on human life are usually simple. A good example of a simple technology with profound historical consequences is hay. Nobody knows who invented hay, the idea of cutting grass in the autumn and storing it in large enough quantities to keep horses and cows alive through the winter. All we know is that the technology of hay was unknown to the Roman Empire but was known to every village of medieval Europe. Like many other crucially important technologies, hay emerged anonymously during the so-called Dark Ages. According to the Hay Theory of History, the invention of hay was the decisive event which moved the center of gravity of urban civilization from the Mediterranean basin to Northern and Western Europe. The Roman Empire did not need hay because in a Mediterranean climate the grass grows well enough in winter for animals to graze. North of the Alps, great cities dependent on horses and oxen for motive power could not exist without hay. So it was hay that allowed populations to grow and civilizations to flourish among the forests of Northern Europe. Hay moved the greatness of Rome to Paris and London, and later to Berlin and Moscow and New York.

But what factor, or combination of factors, may have caused the famine(s) in the Eastern Mediterranean during these decades remains uncertain. Elements that might be considered include war and plagues of insects, but climate change accompanied by drought is more likely to have turned a once-verdant land into an arid semidesert.

Climate change may be far beyond the concerns of people in the midst of a life-and-death emergency, but it might eventually make the Mumbai slums uninhabitable, send enormous new waves of refugees across the Mediterranean, and lead to a worldwide crisis in healthcare.

Nine years later, Britain’s Parliament began canvassing sites for a convict settlement to replace the rebellious American colonies, which had long provided a dumping ground for prisoners sentenced to “transportation.” Parliament sought a “distant part of the Globe, from whence [convicts’] Escape might be difficult,” and where they would be able to “maintain themselves…with little or no aid from the Mother Country.” Joseph Banks recommended Botany Bay, which he said enjoyed a gentle Mediterranean climate and could support “a very large Number of People.

Aristotle, who lived from 384 to 322 BCE, concocted a climate theory to justify Greek superiority, saying that extreme hot or cold climates produced intellectually, physically, and morally inferior people who were ugly and lacked the capacity for freedom and self-government. Aristotle labeled Africans “burnt faces”—the original meaning in Greek of “Ethiopian”—and viewed the “ugly” extremes of pale or dark skins as the effect of the extreme cold or hot climates. All of this was in the interest of normalizing Greek slaveholding practices and Greece’s rule over the western Mediterranean. Aristotle situated the Greeks, in their supreme, intermediate climate, as the most beautifully endowed superior rulers and enslavers of the world. “Humanity is divided into two: the masters and the slaves; or, if one prefers it, the Greeks and the Barbarians, those who have the right to command; and those who are born to obey,” Aristotle said. For him, the enslaved peoples were “by nature incapable of reasoning and live a life of pure sensation, like certain tribes on the borders of the civilized world, or like people who are diseased through the onset of illnesses like epilepsy or madness.”4

The river’s isolation and secrecy, however, were only part of what made it superlative. There was also its vertical drop. The Colorado’s watershed encompasses a series of high-desert plateaus that stretch across the most austere and hostile quarter of the West, an area encompassing one-twelfth the landmass of the continental United States, whose breadth and average height are surpassed only by the highlands of Tibet. Each winter, storms lumbering across the Great Basin build up a thick snowpack along the crest of the mountains that line the perimeter of this plateau—an immense, sickle-shaped curve of peaks whose summits exceed fourteen thousand feet. As the snowmelt cascades off those summits during the spring and spills toward the Sea of Cortés, the water drops more than two and a half miles. That amounts to eight vertical feet per horizontal mile, an angle that is thirty-two times steeper than that of the Mississippi. The grade is unequaled by any major waterway in the contiguous United States and very few long stretches of river beyond the Himalayas. (The Nile, in contrast, falls only six thousand feet in its entire four-thousand-mile trek to the Mediterranean.) Also unlike the Nile, whose discharge is generated primarily by rain, the engine that drives almost all of this activity is snow. This means that the bulk of the Colorado’s discharge tends to come down in one headlong rush. Throughout the autumn and the winter, the river might trickle through the canyonlands of southern Utah at a mere three thousand cubic feet per second. With the melt-out in late May and early June, however, the river’s flow can undergo spectacular bursts of change. In the space of a week, the level can easily surge to 30,000 cfs, and a few days after that it can once again rocket up, surpassing 100,000 cfs. Few rivers on earth can match such manic swings from benign trickle to insane torrent. But the story doesn’t end there, because these savage transitions are exacerbated by yet another unusual phenomenon, one that is a direct outgrowth of the region’s unusual climate and terrain. On

Meritocracy and the Mediterranean climate are by necessity incompatible. I suppose it's the price we pay for having the best olive oil in the world.

The island of Sicily is the largest in the Mediterranean. It has also proved, over the centuries, to be the most unhappy. The stepping-stone between Europe and Africa, the gateway between the East and the West, the link between the Latin world and the Greek, at once a stronghold, observation-point and clearing-house, it has been fought over and occupied in turn by all the great powers that have at various times striven to extend their dominion across the Middle Sea. It has belonged to them all—and yet has properly been part of none; for the number and variety of its conquerors, while preventing the development of any strong national individuality of its own, have endowed it with a kaleidoscopic heritage of experience which can never allow it to become completely assimilated. Even today, despite the beauty of its landscape, the fertility of its fields and the perpetual benediction of its climate, there lingers everywhere some dark, brooding quality—some underlying sorrow of which poverty, Church influence, the Mafia and all the other popular modern scapegoats may be the manifestations but are certainly not the cause. It is the sorrow of long, unhappy experience, of opportunity lost and promise unfulfilled; the sorrow, perhaps, of a beautiful woman who has been raped too often and betrayed too often and is no longer fit for love or marriage. Phoenicians, Greeks, Carthaginians, Romans, Goths, Byzantines, Arabs, Normans, Germans, Spaniards, French—all have left their mark. Today, a century after being received into her Italian home, Sicily is probably less unhappy than she has been for many centuries; but though no longer lost she still seems lonely, seeking always an identity which she can never entirely find.

but especially on the Mediterranean, where all the powers now faced a catastrophe. No one knows what caused it, but it is probable that a synchronicity of climate, natural disaster, pandemics, greed and systemic implosion sparked movements on some faraway steppe that unleashed a stampede migration in which maritime marauders shattered the rich cities of the Mediterranean and western Asia. The raiders sound like Greeks, the Egyptians called them ‘Sea Peoples’ but they came by land too, sporting new iron breastplates and leg greaves, wielding stabbing swords and shields, all made by the smelting of iron ore and meteoric iron to make a stronger metal. Iron had been known for a long time and it is likely that the smelting process developed slowly in many places, starting in India and spreading via the sophisticated blacksmiths of Hatti to Europe and Africa.

In the survey released in February 2020 cited at the beginning of this book, one respondent noted the interrelatedness of the factors involved in our own current world situation, writing: “While extreme climate events are weakening the societal governance and infrastructure, food and water security will become more and more serious, causing large-scale immigration and further inequity. If several geopolitical crises occur in parallel, many states cannot handle the situation properly, due to lack of resources and with the internal conflict, it would cause catastrophic outcomes all over the world.”13 The parallels between events in our modern world and what happened during the Bronze Age Collapse in the Aegean and Eastern Mediterranean were already readily apparent, but now we need also to take into consideration the catastrophic direct effects of the COVID-19 virus and the ripple effects of the contagion on financial and economic systems that went global at about the same time as the release of the survey.

The grape, of a variety known as sultanina, would ultimately grow best in the wet and temperate soil of California. America's region most climatically similar to the Mediterranean. Fairchild's sample from Italy was the Sultanina rosea seedless raisin grape, which was a stronger specimen than a green sultanina that had already made it to California as nursery stock. Regardless of who was first to lay eyes on the sultanina, the variety took little time to grow into the most popular grape in America, adored by winemakers, raisin producers, and people who ate grapes by the fistful.

PEA (PISUM SATIVUM) Peas are one of the ancient crops from the Fertile Crescent of the Middle East, which have been cultivated for around 9,000 years. They quickly spread across Europe and Asia and became a key source of protein in much of northern Europe. Peas are a winter crop in the Mediterranean basin, thriving in the cooler, damper weather, and so they are brilliantly suited to the northern climate.

In each portside town, enticing aromas waft from every harborside taverna, mountaintop inn, and home. Not only do the Greeks appreciate good food, it is central to their culture. Produce markets spill over with fragrant local provender: grapes, cucumbers, lemons, and tomatoes, as well as sardines, shellfish, and lamb. Lunch--usually the largest meal of the day--begins after 2 P.M., and is followed by an ample siesta. The long work day resumes, and dinner begins after 9 P.M. It may last well into the night among friends: a glass of ouzo--accompanied by singing, guitar playing, and dancing--often ends the evening meal, postponing bedtime until the wee hours. Laughter and conversation flavor the food at every meal. The Mediterranean climate is conductive to year-round outdoor eating. In each home, a table on the patio or terrace takes pride of place. Many home cooks build outdoor ovens and prepare succulent roasted meats and flavorful, herb-scented potatoes that soak up the juice of the meat and the spritz of a lemon. Tavernas, shaded by grape arbors, are synonymous with Greece and its outdoor culinary culture. One of the greatest pleasures of the Greek Isles is enjoying a relaxing meal while breathing the fresh sea air and gazing out on spectacular vistas and blue waters.

Climate Italy’s climate varies greatly from north to south. In the Alps, at the top of the boot, snow lingers on the highest peaks throughout the summer. The foot of the boot has hot, dry summers and mild winters. In summer, the temperature can easily reach 90 degrees Fahrenheit (32 degrees Celsius) or higher. This climate draws many northerners to the Mediterranean beaches in the winter. Rome, Italy’s capital, is in the middle of the boot. It’s average high temperature in January is about 52°F (11°C), and its average high temperature in July is 86°F (30°C). In 2003, Italy suffered a heat wave in which the temperature reached 100°F (38°C) or more throughout the summer. An estimated three thousand people, mostly elderly, died. Rain is the heaviest during the fall and winter months. The rainiest areas are in the north. The city of Udine, in the northeast, receives about 60 inches (150 centimeters) of rain a year, but only about 18 inches (46cm) fall on southern Sicily each year.

Comparing African and Egyptian circumstances also points to other reasons why churches survived in some regions and failed in others. From earliest times, Christianity had developed in the particular social and economic world of the Mediterranean and the Near East, and networks of church organization and mission followed the familiar routes of trade and travel. Also, this social world was founded upon cities, which were the undisputed centers of the institutionalized church. Mediterranean Christianity was founded upon a hierarchical system of metropolitans and bishops based in cities: even the name metropolitan suggests a fundamentally urban system. Over time, though, trade routes changed and some cities lost power or vanished altogether. Between the fifth century and the ninth, these changes had a special effect on the Mediterranean, as sea routes declined in importance and states tended to look more inland, to transcontinental routes within Asia and Africa. This process was accelerated by the impact of plague, particularly during the 540s, and perhaps of climate change. Cities like Carthage and Antioch shrank to nothing, while Damascus and Alexandria lost influence before the new rising stars of Baghdad and Cairo.11 These changes coincided with the coming of Islam rather than being caused by that event, but they had immense religious consequences. Churches that remained wedded to the old social order found themselves in growing difficulty, while more flexible or adaptable organizations succeeded. Nestorians and Jacobites coped well for centuries with an Eastern world centered in Baghdad and looking east into Asia. Initially, too, the old urban framework adapted successfully to the Arab conquest, and Christian bishops made their peace quite easily. Matters were very different, though, when the cities themselves were faced with destruction. By the seventh century, the decline of Carthage and its dependent cities undermined the whole basis of the North African church, and accelerated the collapse of the colonial social order. Once the cities were gone, no village Christians remained to take up the slack. The Coptic Church flourished because its network of monasteries and village churches allowed it to withstand changes in the urban system.

the Mediterranean region’s climate started to warm and become wetter starting 18,000 years ago, archaeological sites become more numerous and widespread, creeping into areas now occupied by the desert. The culmination of this population boom was a period called the Natufian, dated to between 14,700 and 11,600 years ago.7 The early Natufian was a sort of golden era of hunting and gathering. Thanks to a benevolent climate and many natural resources, the Natufians were fabulously wealthy by the standards of most hunter-gatherers. They lived by harvesting the abundant wild cereals that naturally grow in this region, and they also hunted animals, especially gazelle. The Natufians evidently had so much to eat that they were able to settle permanently in large villages, with as many as 100 to 150 people, building small houses with stone foundations. They also made beautiful art objects, such as bead necklaces and bracelets and carved figurines, they exchanged with distant groups for exotic shells, and they buried their dead in elaborate graves. If there ever was a Garden of Eden for hunter-gatherers, this must have been it. But then crisis struck 12,800 years ago. All of a sudden, the world’s climate deteriorated abruptly, perhaps because an enormous glacial lake in North America emptied suddenly into the Atlantic, temporarily disrupting the Gulf Stream and wreaking havoc with global weather patterns.8 This event, called the Younger Dryas,9 effectively plunged the world back into Ice Age conditions for hundreds of years. Imagine

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